1.1What you will learn1.21.1 Why we measure1.31.2 Definition of measurement1.41.3 The three elements of any measurement1.51.4 Physical quantities1.62.1 Fundamental physical quantities1.72.2 Derived physical quantities1.82.3 Physics and mathematics1.92.4 Systems of units1.102.5 The International System of Units (SI)1.112.6 Scientists who benefited humanity1.123.1 From the body to the instrument1.133.2 Examples of instruments, old and modern1.143.3 The vernier caliper — measuring length precisely1.15Lesson 4: Standard Units (Length, Mass, Time)1.164.1 The standard of length — the metre1.174.2 The standard of mass — the kilogram1.184.3 The standard of time — the second1.195.1 The idea1.205.2 Getting the unit from the dimensional formula1.215.4 Table of dimensional formulas1.225.5 Rules to remember ("Pay attention")1.236.1 Dimensional homogeneity1.246.3 Limits of the method (important!)1.25Lesson 7: Multiples and Submultiples of Units; Scientific Notation1.268.1 No measurement is perfect1.278.2 Sources of error1.288.3 Precautions when using a metre ruler1.298.4 Direct and indirect measurement1.30Extra worked problems1.31Summary2.1What you will learn2.21.1 Why study motion?2.31.2 Definition of motion2.41.3 Types of motion2.52.1 Why we need velocity2.62.2 Speed and velocity2.72.3 Converting units2.83.1 Uniform and non-uniform (variable) velocity2.93.2 Instantaneous and average velocity2.104.1 How to draw it2.114.2 Reading the displacement–time graph2.125.1 Definition2.135.2 A motion diagram: the car that gains 5 m/s every second2.145.3 Types of acceleration2.156.1 Reading the graph2.166.2 Analysing a multi-stage graph2.176.3 Extension — displacement from the v–t graph2.186.4 Motion (dot) diagrams2.19Short answers to typical discussion questions2.20Summary2.21Key Scientific Tables & Anatomical Diagrams Extracted from Official Curricula3.1What you will learn3.2Introduction3.31.1 What is force?3.41.2 Resultant force3.52.1 Observation and the old belief3.62.2 Statement of the law3.72.3 Consequences of the first law3.82.4 Inertia3.9Lesson 3: Momentum3.104.1 Statement3.114.2 Another statement of the law3.124.3 Definition of the newton3.134.4 Thinking exercise3.144.6 Life applications of the second law (force, time and change of momentum)3.154.7 The first law as a special case of the second3.165.1 Observations3.175.2 Statement3.185.3 Properties of action and reaction3.195.4 Applications3.20Short answers to typical discussion questions3.21Summary4.1What you will learn4.21.1 What is a fluid?4.31.2 Density (ρ)4.41.3 Relative density4.51.5 Applications of density4.6Lesson 2: Types of Liquid Flow4.72.1 Laminar (streamline) flow4.82.2 Turbulent flow4.92.3 Steady flow4.103.1 Volume flow rate and mass flow rate4.113.2 The continuity equation4.123.3 Everyday examples4.133.5 Enrichment: Bernoulli's principle4.144.1 Experiments showing viscosity4.154.2 Explanation: layers of a liquid4.164.3 The coefficient of viscosity (η)4.174.5 Applications of viscosity4.184.6 Think about it4.19Summary5.1What you will learn5.2Overview5.31.1 Definition5.41.2 Enrichment: heel against elephant5.52.1 Observations5.62.2 Deriving P = Pa + ρgh5.72.3 Consequences5.82.5 Balance of two immiscible liquids in a U-tube5.93.1 Atmospheric pressure5.103.2 The mercury barometer (Torricelli)5.113.3 Units of pressure5.123.4 Factors that do not affect the barometer height5.133.6 Enrichment: the ear at heights5.144.1 The manometer5.154.3 Applications of pressure5.165.1 Pascal's principle5.175.2 The hydraulic press5.185.3 Applications5.19Short answers to typical discussion questions5.20Summary6.1What you will learn6.21.1 Molecules in the three states of matter6.31.2 Brownian motion6.41.3 Intermolecular spaces6.5Lesson 2: The Variables of a Gas6.63.1 The experiment6.73.2 Boyle's law6.84.1 Do all gases expand equally?6.94.2 Charles's apparatus6.104.3 Charles's law6.115.1 The experiment6.125.2 Jolly's apparatus6.135.3 The pressure law6.146.1 Absolute zero from Charles's law and from the pressure law6.156.2 Remarks6.166.3 Relation between Celsius and Kelvin6.177.1 Combining the three laws6.187.2 Enrichment: the ideal gas equation6.197.3 Standard temperature and pressure (STP)6.20Summary and relations1.1What you will learn1.2Lesson 1: The Concept of Physical Measurement1.3Lesson 2: Fundamental and Derived Quantities, and Systems of Units1.4Lesson 3: Measuring Instruments1.5Lesson 4: Standard Units (Length, Mass, Time)1.6Lesson 5: Dimensional Formula1.7Lesson 6: Using Dimensions to Test Equations1.8Lesson 7: Multiples and Submultiples of Units; Scientific Notation1.9Lesson 8: Measurement Error1.10Extra worked problems1.11Summary4.1What you will learn4.2Lesson 1: Fluids and Density4.3Lesson 2: Types of Liquid Flow4.4Lesson 3: Flow Rate and the Continuity Equation4.54.1 Experiments showing viscosity4.64.2 Explanation: layers of a liquid4.74.3 The coefficient of viscosity (η)4.84.4 Worked examples4.94.5 Applications of viscosity4.104.6 Think about it4.11Summary5.1What you will learn5.2Overview5.3Lesson 1: Pressure5.42.1 Observations5.52.2 Deriving P = Pa + ρgh5.62.3 Consequences5.72.4 Worked examples5.82.5 Balance of two immiscible liquids in a U-tube5.9Lesson 3: Atmospheric Pressure and the Barometer5.10Lesson 4: The Manometer and Applications of Pressure5.11Lesson 5: Pascal's Principle and the Hydraulic Press5.12Short answers to typical discussion questions5.13Summary| Experiment | Constant | Law |
|---|---|---|
| Volume against pressure | temperature | Boyle’s law |
| Volume against temperature | pressure | Charles’s law |
| Pressure against temperature | volume | Pressure law (Gay-Lussac’s law) |
| Comparison aspect | Main idea | Keywords |
|---|---|---|
| Boyle’s law |
| constanttemperaturevolumefixed |
| • |
| constantfixedmasstemperature |
| or for two states | P₁V₁ = P₂V₂ | P₁V₁P₂V₂ |
| • |
| graphagainstconstantcurve |
| Example 1. | A gas occupies 600 cm3 at 76 cm Hg. It is compressed at constant temperature to 400 cm3. P₂ = P₁V₁/V₂ = 76 × 600/400 = 114 cm Hg | occupiescompressedconstanttemperature |
| Comparison aspect | Main idea | Keywords |
|---|---|---|
| Example 2. | The pressure of a gas is tripled at constant temperature. Its volume becomes one-third | pressuretripledconstanttemperature |
| Example 3. | 8 cm3 of air is at the bottom of a lake at a depth where the total pressure is 3 atm. The temperature is the same at the surface. At the surface (1 atm): V = 3 × 8 = 24 cm3 | bottomlakedepthtotal |
| Example 4 (barometer-tube). |
| holdsatmosphericpressurepushed |
| Comparison aspect | Main idea | Keywords |
|---|---|---|
| Example 2. | 2 litres of a gas at 27 °C (300 K) is heated to 127 °C (400 K) at constant pressure. V₂ = 2 × 400/300 = 2.67 litres | litresheatedconstantpressure |
| Example 3 (find the temperature). | A gas of volume 500 cm3 at 7 °C (280 K) is heated at constant pressure until its volume becomes 750 cm3. T₂ = 280 × 750/500 = 420 K = 147 °C | volumeheatedconstantpressure |
| Example 4. | Show the coefficient. A gas has 200 cm3 at 0 °C and 273.2 cm3 at 100 °C. αv = (273.2 − 200)/(200 × 100) = 3.66 × 10−3 °C−1 ≈ 1/273. | Showcoefficient |
| Comparison aspect | Main idea | Keywords |
|---|---|---|
| The pressure law |
| constantvolumefixedmass |
| Second form (Kelvin scale). |
| similartriangles |
| P / T = constant |
| fixedmassvolume |
| • |
| constantvolumepressurefixed |
| • | Note that the coefficient of volume expansion at constant pressure αv and the coefficient of pressure increase at constant volume βP are equal for all gases: both = 1/273 K−1. | Notecoefficientvolumeexpansion |
| Example 1. | A gas has a pressure of 45 cm Hg at 27 °C (300 K). Its volume is constant. At 127 °C (400 K): P₂ = 45 × 400/300 = 60 cm Hg | pressurevolumeconstant |
| Comparison aspect | Main idea | Keywords |
|---|---|---|
| Example 2. | A sealed container of air is at 0 °C with pressure 80 cm Hg. It is cooled to −91 °C (182 K): P = 80 × 182/273 = 53.3 cm Hg | sealedcontainerpressurecooled |
| Example 3 (car tyre). |
| AfterdrivingAssumingconstant |
| Example 4 (find the temperature). | The pressure of a gas at constant volume rises from 1 atm at 27 °C to 1.5 atm. T₂ = 300 × 1.5 = 450 K = 177 °C | pressureconstantvolumerises |
| Comparison aspect | Main idea | Keywords |
|---|---|---|
| Boyle | V ∝ 1/P (T constant) | constant |
| Charles | V ∝ T (P constant) Combining: V ∝ T/P → PV/T = constant | constantCombining |
| • | For two states of the same mass of gas | statessamemass |
| P₁V₁/T₁ = P₂V₂/T₂ |
| kelvinconsistentunit |
| Special cases |
| constantBoyleCharlespressure |
| Comparison aspect | Main idea | Keywords |
|---|---|---|
| R = 8.31 J/(mol·K) |
| universalconstantmoleamount |
| Example | the volume of one mole of any gas at STP is V = nRT/P = 1 × 8.31 × 273/1.013 × 105 = 0.0224 m3 = 22.4 litres | volumemole0224litres |
| Comparison aspect | Main idea | Keywords |
|---|---|---|
| STP | 0 °C (273 K) and 76 cm Hg (1 atm = 1.013 × 105 Pa) | |
| Example 1 (to STP). | A gas has volume 450 cm3 at 27 °C and 60 cm Hg. Find its volume at STP | volumeFind |
| P₁V₁/T₁ = P₂V₂/T₂ | 60 × 450/300 = 76 × V₂/273 → V₂ = 60 × 450 × 273/(300 × 76) = 323 cm3 | |
| Example 2 (find T). | A gas of 3 L at 2 atm and 27 °C changes to 6 L at 1.5 atm. T₂ = T₁ P₂V₂/(P₁V₁) = 300 × (1.5 × 6)/(2 × 3) = 300 × 1.5 = 450 K = 177 °C | changesP₂V₂P₁V₁ |
| Example 3 (find P). |
| fixedmasscompressedheated |
| Example 4 (gas that escapes). |
| openflaskheatedconstant |
| Comparison aspect | Main idea | Keywords |
|---|---|---|
| Boyle’s Law |
| constanttemperaturevolumefixed |
| Charles’s Law |
| constantpressurevolumefixed |
| Pressure Law (Gay-Lussac’s Law) |
| constantvolumefixedmass |
| Absolute Zero (0 Kelvin / -273.15°C) |
| theoreticaltemperaturevolumeconstant |
| Ideal Gas Equation |
| statecombiningthreeempirical |
| Comparison aspect | Main idea | Keywords |
|---|---|---|
| Boyle’s Law (T = const) | P₁ V₁ = P₂ V₂ | |
| Charles’s Law (P = const) | V₁ / T₁ = V₂ / T₂ (where T = t°C + 273.15) | |
| Pressure Law (V = const) | P₁ / T₁ = P₂ / T₂ | |
| General Combined Gas Law | (P₁ V₁) / T₁ = (P₂ V₂) / T₂ | |
| Ideal Gas Law | P V = n R T = (m / M) R T | |
| Volume Expansion Coefficient | α_v = (Vt – V0) / (V0 × t) = 1 / 273.15 K−1 |
| Comparison aspect | Main idea | Keywords |
|---|---|---|
| • |
| gasesidenticalthermalexpansion |
| Why can gas volume never actually reach zero at absolute zero? | Because real gases condense into liquids and freeze into solids long before reaching 0 K as attractive van der Waals forces overcome kinetic energy | Becauserealgasescondense |
| Why do car tires sometimes burst on hot highways? |
| Frictionraisestemperatureenclosed |
| Gas Law | Constant Parameter | Proportionality | Governing Formula |
|---|---|---|---|
| Boyle’s Law | Temperature (T) | Inverse: P ∝ 1/V | P₁ V₁ = P₂ V₂ |
| Charles’s Law | Pressure (P) | Direct: V ∝ T(K) | V₁ / T₁ = V₂ / T₂ |
| Pressure Law | Volume (V) | Direct: P ∝ T(K) | P₁ / T₁ = P₂ / T₂ |
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